C23A:
Frozen Soil, Its Change, and the Responses and Feedbacks of the Frozen Soil Change in Atmosphere, Hydrology, and Ecosystem II Posters


Session ID#: 8437

Session Description:
Frozen soil is an important component of cryosphere. Atmosphere, frozen soil, water and ecosystem together form a dynamic system that is filled with responses and feedbacks. Distinctive features in atmosphere, hydrology and ecosystems are associated with the frozen soil. For example, at different thawing and freezing stages, soil surface sensible and latent heat fluxes assume dominant roles differently. Permafrost soil limits the interaction between soil surface and deep groundwater due to the hydraulic impedance. In high altitudes, the wetland ecosystem is associated with the permafrost soil. With warming climate, frozen soil degradation has been reported in the high latitudes and altitudes. Components of the dynamic system are expected to alter, and so do the responses and feedbacks among the components. In this session, we welcome studies that focus on the frozen soil modeling and observation, the mechanisms of frozen soil change, and the responses and feedbacks in the dynamic system.
Primary Convener:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Conveners:  Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China, Shilong Piao, Peking University, Beijing, China and Lin Zhao, LZU Lanzhou University, Lanzhou, China
Chairs:  Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Lin Zhao, LZU Lanzhou University, Lanzhou, China
OSPA Liaison:  Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China

Cross-Listed:
  • A - Atmospheric Sciences
  • B - Biogeosciences
  • GC - Global Environmental Change
  • H - Hydrology
Index Terms:

Abstracts Submitted to this Session:

Congrong Yu, Hohai University, Nanjing, China
Andrew Evans, Metropolitan State University of Denver, Denver, CO, United States
Alice Frances Hill, National Institute of Water and Atmospheric Research (NIWA), Nelson, New Zealand, Mark W Williams, Univ Colorado, Boulder, CO, United States and Kurt Chowanski, Institute for Arctic and Alpine Research, Boulder, CO, United States; South Dakota State University, Department of Natural Resource Management, Rapid City, SD, United States
Yingsha Jiang, Northwest Institue of Eco-Environment and Resources, CAS, Lanzhou, China and Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
Xia Li, CAREERI/CAS Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou, China and Yanhong Gao, Northwest Institute of Eco-Environment and Resources, CAS, Lanzhou, China
Lan Cuo, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Fuxin Zhu1, Lan Cuo1, Yongxin Zhang2 and Jing-Jia Luo3, (1)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (2)National Center for Atmospheric Research, Boulder, United States, (3)Bureau of Meteorology, Melbourne, Australia
Sebastian Zubrzycki, University of Hamburg, Hamburg, Germany, Yingzhao Ma, ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China and Yinsheng Zhang, Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Huiyi Bao, University of Tokyo, Bunkyo-ku, Japan
Akihiko Sasaki, Kokushikan University, Setagaya, Tokyo, Japan and Keisuke Suzuki, Shinshu University, Matsumoto, Japan
Sarah Marie Strand and Hanne H. Christiansen, University Centre in Svalbard, Arctic Geology Department, Longyearbyen, Norway

See more of: Cryosphere